1989
DOI: 10.1086/115201
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Various aspects of numerical determination of nutation constants. I - Improvement of rigid-earth nutation

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Cited by 30 publications
(12 citation statements)
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“…The other is to take into account corrections for large coefficients, which are due to a coupling effect between the rotation of the Earth and the revolution of the Moon. Two reconstructions of the nutation for a rigid Earth model were done recently by Zhu and Groten (1989) and Kinoshita and Souchay (1990). For some reasons, explained in detail by Souchay (1993) this last theory looks more accurate and more complete, especially because it includes the planetary effects.…”
Section: Resultsmentioning
confidence: 99%
“…The other is to take into account corrections for large coefficients, which are due to a coupling effect between the rotation of the Earth and the revolution of the Moon. Two reconstructions of the nutation for a rigid Earth model were done recently by Zhu and Groten (1989) and Kinoshita and Souchay (1990). For some reasons, explained in detail by Souchay (1993) this last theory looks more accurate and more complete, especially because it includes the planetary effects.…”
Section: Resultsmentioning
confidence: 99%
“…In addition, the geodynamical ellipticity used is the same as that in Ref. [8] for the sake of comparison, that is…”
Section: Determination Of Constants Related With Nutation Sequence Ofmentioning
confidence: 99%
“…The observation data processing of modern VLBI shows that there exit some differences between theoretic values of nutation and observation data, so the modification of the IAU1980 nutation theory is required. Now there are two rigid Earth nutation theories: the method of analytical mechanics [6,7] and the tidal wave method [8,9] . At present, the analytical mechanics method contains the direct and indirect effects of planets, and considers more perturbation factors, which makes the theory more perfect.…”
Section: Introductionmentioning
confidence: 99%
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“…This nutation model was modified for a deformable Earth by Wahr (1981) and is usually referred to as the standard IAU 1980 nutation series. Later, the rigid Earth nutation was improved by Zhu & Groten (1989), denoted by ZG89, and independently by Kinoshita & Souchay (1990), denoted by KS90, by one order of magnitude to 10 µas for ZG89 and 5 µas for KS90, so that they came up with 262 and 277 nutation terms, respectively. The detailed comparison and discussion between these two models can be found in Souchay (1993).…”
Section: Introductionmentioning
confidence: 99%